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Arctic Oscillation

   Also found in: Acronyms, Wikipedia 0.01 sec.
Arctic Oscillation [¦ärd·ik ‚äs·ə′lā·shən]
(meteorology)
Atmospheric pressure fluctuations (positive and negative phases) between the polar and middle latitudes (above 45° North) that strengthen and weaken the winds circulating counterclockwise from the surface to the lower stratosphere around the Arctic and, as a result, modulate the severity of the winter weather over most Northern Hemisphere middle and high latitudes. Also known as the Northern Hemisphere annular mode.


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Another part is that the so-called Arctic Oscillation of wind patterns over the Arctic Ocean is now in a state that it does not allow build-up of old ice, but immediately flushes most ice into the North Atlantic.
Another part is that the so-called Arctic Oscillation of wind patterns over the Arctic Ocean is now in a state that it does not allow build-up of old ice, but immediately flushes most ice into the North Atlantic.
Natural climatic cycles such as the Arctic Oscillation play a role in year-to-year variations in ice cover.
 
 
 
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